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Arctic sea ice decline contributes to thinning lake ice trend in northern Alaska
被引:23
|作者:
Alexeev, Vladimir A.
[1
]
Arp, Christopher D.
[2
]
Jones, Benjamin M.
[3
]
Cai, Lei
[1
]
机构:
[1] Univ Alaska Fairbanks, Int Arctic Res Ctr, 930 Koyukuk Dr, Fairbanks, AK 99775 USA
[2] Univ Alaska Fairbanks, Water & Environm Res Ctr, Fairbanks, AK 99775 USA
[3] US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA
来源:
ENVIRONMENTAL RESEARCH LETTERS
|
2016年
/
11卷
/
07期
基金:
美国国家科学基金会;
关键词:
Arctic;
sea ice decline;
winter climate;
freshwater ice;
thermokarst lakes;
WATER AVAILABILITY;
COASTAL-PLAIN;
SHALLOW LAKES;
THAW LAKES;
REANALYSIS;
THICKNESS;
COVER;
SLOPE;
MODEL;
SNOW;
D O I:
10.1088/1748-9326/11/7/074022
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Field measurements, satellite observations, and models document a thinning trend in seasonal Arctic lake ice growth, causing a shift from bedfast to floating ice conditions. September sea ice concentrations in the Arctic Ocean since 1991 correlate well (r = +0.69, p < 0.001) to this lake regime shift. To understand how and to what extent sea ice affects lakes, we conducted model experiments to simulate winters with years of high (1991/92) and low (2007/08) sea ice extent for which we also had field measurements and satellite imagery characterizing lake ice conditions. A lake ice growth model forced with Weather Research and Forecasting model output produced a 7% decrease in lake ice growth when 2007/08 sea ice was imposed on 1991/92 climatology and a 9% increase in lake ice growth for the opposing experiment. Here, we clearly link early winter 'ocean-effect' snowfall and warming to reduced lake ice growth. Future reductions in sea ice extent will alter hydrological, biogeochemical, and habitat functioning of Arctic lakes and cause sub-lake permafrost thaw.
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